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排序方式: 共有348条查询结果,搜索用时 31 毫秒
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J.A. Milne 《Livestock Production Science》2005,96(1):3-9
The potential environmental effects of livestock farming are mainly associated with intensification of poultry, pig and dairy cow production systems. The major impacts are mainly caused by housing of livestock, which can lead to air and water pollution associated with nitrogen and phosphorus emissions and losses from manure. European countries regulate the potential for these types of pollution through a number of mechanisms, which have received wide public acceptance. In grazing systems, nitrogen pollution, associated with the use of nitrogen fertilizer, is also the subject of legislation. Perhaps because of this regulatory approach, surveys of the public have found that human food quality and animal welfare are more important issues than effects on air and water quality when considering livestock systems.Variation in stocking rates of grazing ruminants can change the structure and composition of pastures with potential impacts on biodiversity and the production of methane, a greenhouse gas. In European countries, maximum stocking rates have been set to reduce these impacts. Surveys of the European public have suggested that they are willing to pay for the mitigation of these environmental effects but that they also value strongly the cultural component of grazed livestock systems. There are few underlying concepts about how society views the environmental impacts of livestock systems. These are used to conclude that current attitudes are likely to prevail in the next decade. 相似文献
3.
G. F. Difford D. W. Olijhoek A. L. F. Hellwing P. Lund M. A. Bjerring Y. de Haas 《Acta Agriculturae Scandinavica, Section A - Animal Sciences》2018,68(1):25-32
This study assessed the ranking of dairy cows using individual-level correlations for methane (CH4) emission on-farm using sniffers and in respiration chambers. In total 20 lactating dairy cows, ten Holstein and ten Jerseys were recorded using sniffers installed in milking robots for three weeks of lactation and subsequently in respiration chambers (RC) where they were each recorded on three occasions within the RC. Bivariate linear mixed models were used to determine the individual-level correlations (rI) between sniffer and RC phenotypes as proxies for genetic correlations. Despite differences in feeding and management, the predicted CH4 production from sniffers correlated highly with RC CH4 production rI?=?0.77?±?0.18 and CH4 breath concentration correlated nearly as well with RC CH4 production rI?=?0.75?±?0.20. These correlations between sniffers on-farm and RC demonstrate the potential of sniffers measurements as large-scale indicator traits for CH4 emissions in dairy cattle. 相似文献
4.
Methane (CH4) is a potent greenhouse gas and the huge CH4 fluxes emitted from paddy fields can prejudice the eco-compatibility of rice cultivation. CH4 production in submerged rice crops is known to be highly influenced by water temperature. Hence, lowering ponding water temperature (LPWT) could be an option to mitigate CH4 emissions from paddy environments when it is possible either to irrigate with slightly colder water or to increase ponding water depth. However, paddy soil is a complex environment in which many processes are simultaneously influenced by temperature, leading to a difficult prediction of LPWT effects. For this reason, LPWT efficiency is here theoretically investigated with a one-dimensional process-based model that simulates the vertical and temporal dynamics of water temperature in soil and the fate of chemical compounds that influence CH4 emissions. The model is validated with literature measured data of CH4 emissions from a paddy field under time-variable temperature regime. Based on modeling results, LPWT appears promising since the simulated reduction of CH4 emissions reaches about −12% and −49% for an LPWT equal to −5 °C during the ripening stage only (last 30 days of growing season, when rice is less sensitive to temperature variations) and −2 °C over the whole growing season, respectively. LPWT affects CH4 emissions either directly (decreasing methanogenic activity), indirectly (decreasing activity of bacteria using alternative electron acceptors), or both. The encouraging results provide the theoretical ground for further laboratory and field studies aimed to investigate the LPWT feasibility in paddy environments. 相似文献
5.
This study aimed to evaluate the effect of different dose levels of aguamiel (Agave atrovirens) on in vitro cecal gas, methane (CH4), and carbon dioxide (CO2) productions of five forage species (Avena sativa [hay]), Moringa oleifera, Caesalpinia coriacea, Salix babylonica, and Eichhornia crassipes using inocula from the horse. The forage samples were incubated with three doses of aguamiel: 0, 34, and 68 μg of aguamiel/g dry matter (DM) of substrate. Cecal inocula were collected from four adult female Criolla horses (3–4 years of age and weighing 300 ± 15.0 kg) grazed on native grasses for about 8 hours without supplementation. Forage type affected (P < .001) cecal asymptotic, rate and lag time of gas, CH4 and CO2 productions (mL/g DM), pH and DM degradability. Aguamiel dose had linear and quadratic effects (P < .05) on the asymptotic and rate of CH4 productions and rate and lag time of CO2 productions (mL/g DM). Forage type × aguamiel dose interactions were significant (P < .05) for asymptotic, rate and lag time of gas, and CH4 and CO2 productions (mL/g DM). Forage species effects were pronounced (P < .05) on CH4 and CO2 productions (mL/g incubated and degraded DM) and proportional CH4 production at all hours of incubation, except for CO2 production (mL/g incubated DM). Aguamiel dose affected (P < .05) CO2 production (mL/g incubated DM) and proportional CO2 production at the incubated hours. Forage type × aguamiel dose interactions were observed (P < .05) for CO2 production (mL/g incubated DM) and proportional CO2 production at the incubated hours but had no impact on CH4 production. It is concluded that addition of aguamiel to five forage species affected fermentation kinetics of gas production resulting in different in vitro cecal gas, CH4 and CO2 productions from these substrates. 相似文献
6.
一种新的厌氧污泥比活性试验测定法 总被引:2,自引:0,他引:2
本文介绍了一种以医用血清瓶作发酵瓶、用医用注射器来量测所产沼气的厌氧污泥比活性试验测定法。实践表明此法简单实用、快速准确。 相似文献
7.
不同生物质炭输入水平下旱作农田温室气体排放研究 总被引:4,自引:0,他引:4
在陇中黄土高原干旱半干旱区,采用小区定位试验,对不同生物质炭输入水平下春小麦农田土壤温室气体(CO_2、N_2O和CH_4)的排放通量进行全生育期连续观测,并分析其影响因子。结果表明:6个生物质炭输入水平处理下[0 t·hm~(-2)(CK)、10 t·hm~(-2)、20 t·hm~(-2)、30 t·hm~(-2)、40 t·hm~(-2)、50 t·hm~(-2)],旱作农田土壤在春小麦全生育期内均表现为CH_4弱源、N_2O源和CO_2源。全生育期各处理CH_4平均排放通量依次为:0.005 7 mg·m~(-2)·h~(-1)、0.0047 mg·m~(-2)·h~(-1)、0.003 6 mg·m~(-2)·h~(-1)、0.003 3 mg·m~(-2)·h~(-1)、0.002 7 mg·m~(-2)·h~(-1)和0.000 4 mg·m~(-2)·h~(-1),N_2O平均排放通量依次为:0.230 5 mg·m~(-2)·h~(-1)、0.144 1 mg·m~(-2)·h~(-1)、0.135 3 mg·m~(-2)·h~(-1)、0.098 9 mg·m~(-2)·h~(-1)、0.125 0 mg·m~(-2)·h~(-1)和0.151 3mg·m~(-2)·h~(-1),CO_2平均排放通量依次为:0.449 2μmol·m~(-2)·s~(-1)、0.447 0μmol·m~(-2)·s~(-1)、0.430 3μmol·m~(-2)·s~(-1)、0.391 4μmol·m~(-2)·s~(-1)、0.408 0μmol·m~(-2)·s~(-1)和0.416 4μmol·m~(-2)·s~(-1)。土壤CH_4排放通量随生物质炭输入量的增加而减小;当生物质炭输入量小于30 t·hm~(-2)时,土壤N_2O、CO_2排放通量随其输入量增加而显著减小,但当其输入量超过30 t·hm~(-2)时,N_2O、CO_2排放通量则呈显著增大趋势。各处理在5~15 cm土层平均土壤温度差异显著(P0.05),在5~10 cm土层平均土壤含水量差异显著(P0.05),土壤温度及含水量受生物质炭影响明显;且CK处理不同土层的土壤温度及含水量波动最大,生物质炭输入可在一定程度上降低不同土层土壤的水热变化幅度;N_2O、CO_2排放通量与10~15 cm土层土壤温度呈显著性负相关,与20~25 cm土壤温度呈显著性正相关;CH_4平均排放通量与5~10 cm土层土壤温度呈显著性负相关,与其含水量呈显著性正相关;N_2O平均排放通量与15~20 cm土层土壤温度呈显著性正相关;CH_4、N_2O、CO_2平均排放通量与0~5 cm土层土壤水分呈显著性负相关。生物质炭的输入能够减小温室气体的排放,且会因其输入量的不同而异,因此适量应用生物质炭有利于旱作农田生育期内增汇减排。 相似文献
8.
Tillage changes soil environmental conditions and controls the distribution of residues in the soil, both actions that affect the production and emission of soil biogenic gases (CO2, N2O, and CH4). The objective of this study was to determine how tillage-induced environmental conditions and substrate quality affect the mineralization rate of easily metabolizable compounds and the subsequent production of these gases. Carbon compounds, with and without nitrogen, were applied to soil cropped to maize under tilled and no-till systems. Following substrate application in the spring and summer, biogenic gases were measured periodically at the soil surface (flux) and within the profile (concentration) at 10-, 20-, and 30-cm depths (i.e., within, at the bottom of, and below the plough layer). Strong CO2 and N2O responses to sucrose and glycine in both the field and the laboratory indicate that the soil was C- and N-limited. Surface fluxes of CO2 and N2O were greater in soils amended with glycine than with sucrose and were greater in tilled than no-till soils. Transient emission of CH4 following the addition of glycine was observed and could be attributed to inhibition of N mineralization and nitrification processes on CH4 oxidation. Laboratory and field measurements indicated that the larger substrate-induced CO2 emission from the tilled soils could not be attributed to differences in the total biomass or the basal respiratory activity of the soils. Thus, there appears to be no underlying difference in the functional capacity of the microbial communities under different tillage regimes. Comparison of gas profiles indicates relative accumulation of CO2 at depth in soils under no-till, as well as greater decline in profile CO2 content with time in the tilled compared to the no-till soil. These results support the conclusion that greater CO2 efflux from the tilled soils resulted from more rapid gas diffusion through the profile. Hence, the observed differences in gas fluxes between tilled and no-till soils can be attributed to differences in physical environment. 相似文献
9.
Naoki Harada Shigeto Otsuka Masaya Nishiyama Satoshi Matsumoto 《Biology and Fertility of Soils》2005,41(1):46-51
A pot experiment was conducted to investigate the influences of indigenous phototrophs on methane (CH4) emissions from a paddy soil where rice straw was incorporated or was surface-applied. During the cultivation, half of the pots were covered with aluminum foil, except for the minimum space for rice plants, to prevent ambient light reaching the floodwater or the soil surface. Growth of oxygen-producing phototrophs was hardly observed in the unilluminated plots, whereas intensive growth of algae, duckweed and hydrophytes was found in the illuminated ones. Plant growth was not affected by the different treatments. Seasonal changes in CH4 emission determined by a closed chamber method indicated that illumination had no or only minor effects on CH4 emissions when rice straw was incorporated or was not applied, but significantly reduced CH4 emissions when rice straw was surface-applied. Methanogenesis occurring in the soil-floodwater interface was further investigated in two lab-scale model experiments measuring methanogenic activity. As a result, more activated methanogenesis was found in the surface-applied rice straw and the soil around the straw compared with the soil incubated without rice straw. The magnitude of the methanogenic activity in the rice straw incubated under illuminated conditions was significantly lower than that incubated in the dark. Consequently, this study demonstrates that methanogenesis in paddy soil occurs even in the soil-floodwater interface if plant residues like rice straw exist, and such methanogenesis is likely to be suppressed by growth of indigenous phototrophs under illumination. 相似文献
10.